Zobrazeno 1 - 10
of 108
pro vyhledávání: '"Planetary accretion"'
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Early in the history of the solar system, planetesimals were differentiated into metallic cores. In some planetesimals, this differentiation took place by percolation of the denser core forming liquid through a lighter solid silicate matrix. A key fa
Externí odkaz:
https://doaj.org/article/a0370a55725840ec8a6f2ac3c9c638a6
Autor:
Halliday, Alex N., Lee, Der-Chuen, Porcelli, Don, Wiechert, Uwe, Schönbächler, Maria, Rehkämper, Mark
Publikováno v:
Philosophical Transactions: Mathematical, Physical and Engineering Sciences, 2001 Oct . 359(1787), 2111-2135.
Externí odkaz:
https://www.jstor.org/stable/3066278
Autor:
Timothy L. Grove, Max Collinet
Publikováno v:
Geochimica et Cosmochimica Acta. 277:334-357
We present the results of melting experiments on a suite of carbonaceous and ordinary chondritic compositions (CV, CM, CI, H and LL) performed at low pressure (0.1–13.1 MPa) and over a range of oxygen fugacity (log fO2 − (log fO2)IW = −2.5 to
Autor:
Heon-Young Chang, Chul-Sung Choi
Publikováno v:
Journal of Astronomy and Space Sciences, Vol 19, Iss 3, Pp 181-186 (2002)
We study a role of the proto-accretion disk during the formation of the planetary system, which is motivated with recent X-ray observations. There is an observational correlation of the mass of extrasolar planets with their orbital period, which also
Externí odkaz:
https://doaj.org/article/dd550171728d4615bb85d8c49ff19da1
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America
During the formation of terrestrial planets, volatile loss may occur through nebular processing, planetesimal differentiation, and planetary accretion. We investigate iron meteorites as an archive of volatile loss during planetesimal processing. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15694bf056458da79c1ec8e34d62a316
http://arxiv.org/abs/2104.02706
http://arxiv.org/abs/2104.02706
Autor:
Kubik, Edith
Publikováno v:
Sciences de la Terre. Université de Paris, 2020. Français. ⟨NNT : 2020UNIP7097⟩
The accretion of volatile elements on Earth continues to be debated despite intense research focusing on the topic. Geochemical and cosmochemical observables have been explained by a variety of scenarios ranging from (1) an accretion of the volatile
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0d8c713df9da29a44c1a1f086a028a83
https://tel.archives-ouvertes.fr/tel-03249578
https://tel.archives-ouvertes.fr/tel-03249578
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Early in the history of the solar system, planetesimals were differentiated into metallic cores. In some planetesimals, this differentiation took place by percolation of the denser core forming liquid through a lighter solid silicate matrix. A key fa
Autor:
Max Collinet, Timothy L. Grove
Acapulcoites-lodranites, ureilites, brachinites, brachinite-like achondrites and winonaites are the main groups of primitive achondrites. They are variably depleted in incompatible lithophile elements (Al, Na, K and rare earth elements) and siderophi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cab6054b103bdd45d4739e288bb1ccee
https://elib.dlr.de/137523/
https://elib.dlr.de/137523/
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